Comments:
multiple grade controls account for large majority of slope (GIS calc 3.4 pct slope); pockets of floodplain otherwise indicate a C-type stream, but semi-confined valley and repeated large storms (2009, 2010 localized flash floods, relatively limited impacts of 2011 TS Irene) contribute to movement of large materials lending to step-pool bedform. w/d ratio is within range for E-type stream, but have used +/- .2 factor to characterize as C-type due to relatively low sinuosity and nature of geologic materials and substrate.
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